Tools such as sonar mapping, geologic sampling, and paleomagnetism studies were used to provide evidence for seafloor spreading. Sonar mapping allowed for the creation of detailed maps of the ocean floor, revealing features such as mid-ocean ridges and deep-sea trenches. Geologic sampling involved collecting rock samples from the ocean floor to study their age and composition. Paleomagnetism studies focused on analyzing the alignment of magnetic minerals in rocks, providing evidence of past changes in Earth's magnetic field that support the idea of seafloor spreading.
the only thing the incas used for tools was clay.they used it for building houses,streets and pottery
What we can tell about early people from the tools they used is that they were very resourceful in creating the tools that they needed to get jobs accomplished.
lots of different tools.
Yes the stone age was the time when they used stones as tools
The Incas used tools made of stone, bronze, and wood for various purposes like agriculture, building constructions, and metalworking. Some common tools included stone masonry tools, farming implements like hoes and digging sticks, and metalworking tools for creating jewelry and weapons.
No
seafloor spreading
The name of the research vessel that was used in proving the seaflor spreading was the vessel Pioneer. It is a marine magnetometer. mikee...=)
Harry Hess
New material is added to the sea floor when sea floor spreading occurs. When the iron cools it is magnetized by the magnetic field of the earth.
1960 (although Hess' paper built upon Alfred Wegener's theory of continental drift , proposed in 1915).
A magnetometer is a device that is used to detect magnetic fields on the seafloor. It was invented by Sheldon Breiner.
Using sonar, oceanographers were able to show that the edges of the continental shelves matched.
Sonar is used to map the seafloor.
Fossils, Climate, and Sea-Floor Spreading
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.
landsat satellite